Abstract

Significant resources have been spent in collecting and storing large and heterogeneous radar datasets during expensive Arctic and Antarctic fieldwork. The vast majority of data available is unlabeled, and the labeling process is both time-consuming and expensive. One possible alternative to the labeling process is the use of synthetically generated data with artificial intelligence. Instead of labeling real images, we can generate synthetic data based on arbitrary labels. In this way, training data can be quickly augmented with additional images. In this research, we evaluated the performance of synthetically generated radar images based on modified cycle-consistent adversarial networks. We conducted several experiments to test the quality of the generated radar imagery. We also tested the quality of a state-of-the-art contour detection algorithm on synthetic data and different combinations of real and synthetic data. Our experiments show that synthetic radar images generated by generative adversarial network (GAN) can be used in combination with real images for data augmentation and training of deep neural networks. However, the synthetic images generated by GANs cannot be used solely for training a neural network (training on synthetic and testing on real) as they cannot simulate all of the radar characteristics such as noise or Doppler effects. To the best of our knowledge, this is the first work in creating radar sounder imagery based on generative adversarial network.

Highlights

  • Ice loss in Greenland and Antarctica has accelerated in recent decades

  • The images used in this research are CReSIS standard output products collected with a radar depth sounder (RDS) from the years 2009 to 2017

  • We developed an architecture based on the CycleGAN network to generate synthetic radar depth sounder images

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Summary

Introduction

Ice loss in Greenland and Antarctica has accelerated in recent decades. Melting polar ice sheets and mountain glaciers have considerable influence on sea-level rise (SLR) and ocean currents; potential floods in coastal regions could put millions of people around the world at risk. Precise calculation of ice thickness is very important for sea level and flood monitoring. The shape of the landscape beneath the thick ice sheets is an important factor in predicting ice flow. Radars are one of the most important sensors that can penetrate through ice and give us information about the ice thickness. Several semi-automated and automated methods exist for layer finding and estimating ice thickness in radar images [1,2,3,4,5,6]. Crandall et al [1] used probabilistic graphical models for detecting the ice layer boundary in echogram images from Greenland and Antarctica. Mitchell et al [3] used a level set technique for estimating bedrock and surface layers. For every single image, the user needs to re-initialize the curve manually and as a result, the method is quite slow and was applied only to a small dataset

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